• 암석학회지
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• 제5권2호
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• pp.168-187
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• 1996

연구지역인 장군봉-삼근리 일대 선캠브리아대의 암석들에는 고생대 이전에 적어도 세 차례의 광역 변성 작용이 있었다. 연구 지역이 고생대 변성 퇴적암류는 고생대 이후 세 차례의 변성 작용을 받았으며 그 첫 번째는 저압형의 광역 변성 작용이고 두 번째는 춘양 화강암이 관입에의해 형성된 접촉 변성 작용이며 세 번째는 장군봉 남쪽의 드러스트에 의해 중압형 변성 작용이다. 그 첫 번째의 변성 작용은 본 지역을 우세하게 지배하는 변성 분대를 형성시켰으며 변성 정도가 남쪽에서부터 북쪽으로 클로리토이드대, 십자석대, 석류석대, 십자석+흑운모대, 홍주석+흑운모대의 순서로 증가한다. 고생대 이후 두 번째의 접촉 변성 작용은 춘양 화강암 주변의 선캠브리아대의 태백산 편암 복합체와 고생대 변성 퇴적암류에 동시에 영향을 주었으며 접촉부 주위에 매우 좁게 한정되어 인지된다. 세 번째 있었던 변성 작용은 남정석을 형성시켰으며 장군봉 남쪽에 동서 방향으로 발달한 드러스트 주변 지역에 한정되어 영향을 미쳤다.

• 한국환경농학회지
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• 제34권3호
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• pp.168-177
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• 2015

BACKGROUND: In recent year, there has been great concern regarding agricultural land uses and their importance for the conservation of biodiversity. Rice fields are managed unique wetland for wildlife, especially waterbirds. A comprehensive monitoring of the waterbird assemblage to understand patterning changes was attempted for rice ecosystem in South Korea. This rice ecosystem has been recognized as one of the most important for waterbirds conservation. METHODS AND RESULTS: Biweekly monitoring was implemented for the 4 years from April 2009 to March 2010, from April 2011 to March 2014. 32 species of waterbirds were observed. Self-organizing map (SOM) and random forest were applied to the waterbirds dataset to identify the characteristics in waterbirds distribution. SOM and random forest analysis clearly classified into four clusters and extract ecological information from waterbird dataset. Waterbird assemblages represented strong seasonality and habitat use according to waterbird group such as shorebirds, herons and waterfowl. CONCLUSION: Our results showed that the combination of SOM and random forest analysis could be useful for ecosystem assessment and management. Furthermore, we strongly suggested that a strict management strategy for the rice fields to conserve the waterbirds. The strategy could be seasonally and species specific.

• 한국습지학회지
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• 제8권3호
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• pp.51-65
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• 2006

연구지역에서 2003년 8월에 199개 정점에서 표층퇴적물을 채취하여 분석하였다. 표층 퇴적물은 6개의 퇴적상으로 구성되어 있었다. 일반적으로 모래 펄 퇴적물이 강화 남단 갯벌에서 우세하였고 모래 퇴적물은 강화도 서부의 수로와 조하대에서 우세하였다. 이 지역의 1997년 퇴적상과 비교하여 모래펄 퇴적물은 갯벌의 동쪽으로 확장 되었다. 강화 남단 갯벌과 주변부 30 정점의 표층퇴적물에서 살아있는 유공충 34종을 포함하여 총 61종의 유공충이 확인되었다. 살아있는 유공충에서는 Ammonia beccarii와 Elphidium etigoense, 전체군집에서는 Ammonia beccarii, Elphidium etigoense, Jadammina sp.와 Textularia earlandi가 연구지역에 넓게 분포한다. 일반적으로 개체수와 종 다양성은 갯벌의 서부에서 상대적으로 높은 수치를 나타냈다. 전체 유공충 군집의 집괴분석 결과 4개의 생물상으로 구분되었다. 생물상 1은 강화 남단의 동부 갯벌, 생물상 4는 강화 남단의 서부 갯벌의 저서환경을 나타냈다. 생물상 3은 생물상 1과 4의 전이환경으로 보여 진다.

• 한국광물학회지
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• 제10권1호
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• pp.33-44
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• 1997

The reaction path of water-gneiss in 200m borehole at the Soorichi site of Yugu Myeon, Chungnam was simulated by the EQ3NR/EQ6 program. Mineral composition of borehole core and fracture-filling minerals, and chemical composition of groundwater was published by authors. In this study, chemical evolution of groundwater and formation of secondary minerals in water-gneiss system was modelled on the basis of published results. The surface water was used as a starting solution for reaction. Input parameters for modelling such as mineral assemblage and their volume percent, chemical composition of mineral phases, water/rock ratio reactive surface area, dissolution rates of mineral phases were determined by experimental measurement and model fit. EQ6 modelling of the reaction path in water-gneiss system has been carried out by a flow-centered flow through open system which can be considered as a suitable option for fracture flow of groundwater. The modelling results show that reaction time of 133 years is required to reach equilibrium state in water-gneiss system, and evolution of present groundwater will continue to pH 9.45 and higher na ion concentration. The secondary minerals formed from equeous phase are kaolinite, smectite, saponite, muscovite, mesolite, celadonite, microcline and calcite with uincreasing time. Modeling results are comparatively well fitted to pH and chemical composition of borehole groudwater, secondary minerals identified and tritium age of groundwater. The EQ6 modelling results are dependent on reliability of input parameters: water-rock ratio, effective reaction surface area and dissolution rates of mineral phases, which are difficult parameters to be measured.

• 한국해양학회지
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• 제30권2호
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• pp.69-76
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• 1995

오끼나와 해곡의 남쪽 해저 2051 m에서 채취된 저탁류 퇴적물(RN88-PC5)에 대하여 조사하였다. 반원양성 점토질 퇴적물과 천해에서 운반된 사질퇴적물 사이에는 저저성 유공충의 조성, 입도조성 및 화학적 원소의 조성 등에서 현저한 퇴적학적 특성의 차이 를 보인다. 저탁류 퇴적물인 사질퇴적물에 있어서는 점토질 퇴적물에는 포함되어 있지 않은 전형적인 신호초 해역의 유공충을 다량으로 함유하고 있는 것으로 보아 천해에서 유입된 퇴적물임이 거희확실하다. 이들 사질퇴적물은 저탁류와 관련되어 운반 되었으 며, 사질퇴적물과 점토질퇴적물 사이에는 다른 퇴적학적인 기작이 작용되었음을 시사 한다. /SUP 14/C 연대측정 결과와 유공충의 안정 산소동위원소값의 변화는 과거 약 1 만년으로부터 현재에 이르기까지 포층해수의 점진적인 온난화 경향을 보인다. 또한 Termination 1b의 기록을 보일 뿐만 아니라 약 2천년전과 7천년전의 2회에 걸친 담수 유입의 증거도 보여진다.

• 생태와환경
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• 제36권2호통권103호
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• pp.117-123
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• 2003

러시아의 바이칼 호수에서의 식물성 플랑크톤을 함유한 mesocosm 실험, 물벼룩(Daphnia magna)과 클로렐라(Chlorella vulgaris)를 함유한 microcoms 실험 결과에 따르면 펩톤, 디젤오일, odiphenol 및 $CdCl_2$을 mesocosm에 첨가하였을 때, 또 페놀, $CoCl_2$및 $CuSO_4$를 microcosm에 첨가함에 따라 구조 엑서지 (structrural exergy)가 감소하였다. 오염된 지역의 수계 생태계에서는 각 구성성분의 생물량과 총 생물량의 변화 보다는 구조 엑서지의 변화가 훨씬 컸다. 또, 바이칼 호수 주변의 Baikalsk Pulp and Paper Combine으로부터 나오는 배출수의 영향을 받는 지역과 청정지역의 benthos의 엑서지를 비교해 보면, 오염된 지역에서 군집의 구조 엑서지가 급격히 감소하였다. 이러한 결과는 구조 엑서지가 생태계의 건강성을 반영하는 척도로서 이용될 수 있음을 보여주는 것이다.

• 생태와환경
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• 제42권1호
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• pp.95-106
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• 2009

The Shihwa constructed wetland was established for the treatment of severely poluted water from Banwoul, Donghwa and Samhwa streams. This study was focused on investigating the structure of epiphytic diatom communities on reed (Phragmites communis) planting area at Banwoul high wetland (3 stations) and low wetland (3 stations) from March to October 2005. The concentration of T-N of inlet stations from the streams were decreased by flowed through the wetland, but the concentration of T-P were increased at outflow part. Epiphytic diatoms on the reed were a total 109 taxa which were composed of 103 species, 5 varieties, 1 unidentified species. The standing crops were rapidly decreasing tendency from spring to autumn but chlorophyll-a concentration were showed a very irregulated changes. Dominant species were 6 taxa which were Achnanthes minutissima in the early investigation, and were changed to the genus Navicula and the genus Nitzschia in the summer. DAIpo were ranged the values of $20.2{\sim}51$, which were mesosaprobic states at the high wetland and ranged the values of $12.4{\sim}52$, which were polysaprobic to mesosaprobic states at the low wetland. TDI were ranged the values of $28.8{\sim}94.5$, which were oligotrophic to eutrophic state at the high wetland and ranged the values of $33.3{\sim}89.7$ which were mesotrophic to eutrophic states at the low wetland. The healthy assessment (DAIpo and TDI) of water ecosystem were showed clean-bad from spring to autumn. These epiphytic diatom communities were determinated by the biological factor such as the growth of reed and the physical factors such as water temperature, light penetration and SS and so on.

• 생태와환경
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• 제41권1호
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• pp.111-115
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• 2008

Direct effects of zooplankton grazing activities on the natural assemblage of bacterioplankton and algae were evaluated at monthly intervals, from June to October of 2000, in the middle part of the River Spree, Germany. We quantified bacterioplankton, algae, zooplankton abundance and measured carbon ingestion rates (CIRs) by zooplankton according to two zooplankton size classes: (i) micro zooplankton (MICZ), ranging in size from 30 to $150{\mu}m$ and including rotifers and nauplii, excluding protozoans and (ii) macrozooplankton (MACZ), larger than $150{\mu}m$ and including cladocerans and copepods. CIRs were measured using natural bacterial and algae communities in the zooplankton density manipulation experiments. Algae biomass (average${\pm}$SD: $377{\pm}306{\mu}gC\;L^{-1}$, n=5) was always higher than bacterial biomass ($36.7{\pm}9.9{\mu}gC\;L^{-1}$, n=5). Total zooplankton biomass varied from 19.8 to $137{\mu}gC\;L^{-1}$. Total mean biomass of zooplankton was $59.9{\pm}52.5{\mu}gC\;L^{-1}$ (average${\pm}$SD, n=5). Average MICZ biomass ($40.2{\pm}47.6{\mu}gC\;L^{-1}$ n=5) was nearly twofold higher than MACZ biomass ($19.6{\pm}20.6{\mu}gC\;L^{-1}$ n=5). Total zooplankton CIRs on algae (average${\pm}$SD: $56.6{\pm}26.4{\mu}gC\;L^{-1}\;day^{-1}$) were $\sim$fourfold higher than that on bacteria $(12.7{\pm}6.0{\mu}gC\;L^{-1}\;day^{-1})$. MICZ CIRs on bacteria $(7.0{\pm}2.8{\mu}gC\;L^{-1}\;day^{-1})$ and algae $(28.6{\pm}20.6{\mu}gC\;L^{-1}\;day^{-1})$ were slightly higher than MACZ CIRs. On average, MICZ accounted for 55.6 and 50.5% of total zooplankton grazing on bacteria and algae, respectively. Considering the MICZ and MACZ CIRs, the relative role of transferring carbon to higher trophic levels were nearly similar between both communities in the lake-river ecosystem.

• 자원환경지질
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• 제21권3호
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• pp.287-307
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• 1988

The Cheongju gold-silver mine is located at approximately $36^{\circ}28^{\prime}$north latitude and $127^{\circ}31^{\prime}$ east longitude in the Cheongju City of the Chung cheong bug Do, South Korea. Gold-Silver bearing hydrothermal quartz veins, occur in Cheongju Granit of Jurassic age. K-Ar isotope data for sericite in quartz vein indicate that the Au-Ag mineralization took place in early Cretaceous ($97.5{\pm}2.18$ MA. Park, et ai, 1986). Three stage of mineralization recognized anre, from early to later, (I) Sulide stage: pyrite, arsenopyrite, pyrrhotite (Hpo), sphalerite, chalcopyrite, electrum and quartz (II) Electrum stage: pyrite, sphalerite, galena, chalcopyrite, electrum and quartz. (III) Silver mineral stage: pyrite, marcasite, pyrrhotite (Mpo), sphalerite, galena, electrum, native silver argentite, fluorite, calcite and quartz. In this paper, mode of occurrences and chemical compositions of electum and native silver have been investigated by means of microscope and EPMA. Electron probe microanalysis shows that an individual grain of electrum is almost homogeneous in composition. Silver content of electrum ranges from 44.7-67.1 atom.%. Gold content of native silver ranges below 0.2 atom. %. Vicker's hardness number (VHN) of electrum and native silver ranges $78.2-81.8kg/mm^{2}$ respectively. The filling temperature of fluid inclusions in quartz ranges from $130-280^{\circ}C$. On the basis of arsenpyrite geothemometer, the equilibrium temperature and sulfur fugacity of the pyrite-arsenopyrite-pyrrhotite(Hpo) assemblage is assumed to be in ange from $300-310^{\circ}C$ and $10^{-10}$ to $10^{-11}$ atm. The estimated ore reserviors on Cheongju mine area are calculated to 8000 T/M, averaing 8.6g/t Au, 27.8 g/t Ag, 1.25% Pb, l.65% Zn.

• Parasites, Hosts and Diseases
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• 제57권5호
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• pp.531-536
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• 2019

Cryptosporidium parvum and Giardia duodenalis are the main diarrhea-causing parasitic pathogens; however, their prevalence in Korea is unknown. Here, we conducted a survey to determine the prevalence and genotype distribution of these 2 pathogens causing acute diarrhea in 8,571 patients hospitalized in 17 Regional Institute of Health Environment sites in Korea, during 2013-2016. C. parvum and G. duodenalis were detected and genotyped by nested PCR, and the isolate were molecularly characterized by sequencing the glycoprotein 60 (Gp60) and ${\beta}-giardin$ genes, respectively. The overall prevalence of C. parvum and G. duodenalis was 0.37% (n=32) and 0.55% (n=47), respectively, and both pathogens were more prevalent in children under 9 years old. Molecular epidemiological analysis showed that the C. parvum isolates belonged to the IIa family and were subtyped as IIaA13G2R1, IIaA14G2R1, IIaA15G2R1, and IIaA18G3R1. Analysis of the ${\beta}-giardin$ gene fragment from G. duodenalis showed that all positive strains belong to assemblage A. This is the first report on the molecular epidemiology and subtyping of C. parvum and G. duodenalis in such a large number of diarrheal patients in Korea. These results highlight the need for continuous monitoring of these zoonotic pathogens and provide a basis for implementing control and prevention strategies. Further, the results might be useful for epidemiological investigation of the source of outbreak.